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Journal articles on the topic 'Wadi Hammamat'

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Published: 4 June 2021
Last updated: 4 February 2022

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1

GOEDICKE, H. "Two Mining Records from the Wadi Hammamat." Revue d'Égyptologie 41 (January 1, 1990): 65–93. http://dx.doi.org/10.2143/re.41.0.2011313.

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2

Gasse, Annie. "Wadi Hammamat on the Road to Punt." Abgadiyat 11, no. 1 (May 12, 2016): 44–50. http://dx.doi.org/10.1163/22138609-90000041.

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3

Hikade, Thomas. "Expeditions to the Wadi Hammamat during the New Kingdom." Journal of Egyptian Archaeology 92, no. 1 (December 2006): 153–68. http://dx.doi.org/10.1177/030751330609200105.

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4

Sweeney, Deborah. "Self-Representation in Old Kingdom Quarrying Inscriptions at Wadi Hammamat*." Journal of Egyptian Archaeology 100, no. 1 (January 2014): 275–91. http://dx.doi.org/10.1177/030751331410000115.

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5

Bloxam, Elizabeth. "‘A Place Full of Whispers’: Socializing the Quarry Landscape of the Wadi Hammamat." Cambridge Archaeological Journal 25, no. 4 (October 15, 2015): 789–814. http://dx.doi.org/10.1017/s0959774315000426.

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The wealth of inscriptions at the Wadi Hammamat greywacke quarries (Egyptian Eastern Desert) have made it a key place to pursue enquiries about the social organization of expeditions to procure resources. Analysis of this textual material alone has, however, given us only a partial view of the social milieu that maintained quarrying from the fourth millennium bc to the fifth century ad. This article presents a fresh perspective on Egyptian quarrying that aims to balance the more accepted (and persistent) perceptions of overriding state control of these activities with viewpoints gained from recent archaeological survey of the Wadi Hammamat quarries. Practically and theoretically, a holistic approach is taken that contextualizes the textual sources and other elements of the archaeological record within the quarry landscape as a series of material complexes. Cross-cultural and comparative approaches to interpreting the data have enabled both reappraisal and augmentation of the ways in which we understand the social interplay between local and regional kin-groups within notions of state control of these activities. The article argues for the essential roles played by kinship ties and linkages to place, through the continual inscribing of names, as parts of the underlying human narrative that maintained quarrying here for generations.
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6

Mira, Hamed Ibrahim, Hussein Kamal Hussein, Sameh Zakaria Tawfik, and Neveen Salah Abed. "Stream Sediments Geochemical Exploration in Wadi El Reddah area, Northeastern Desert, Egypt." Mediterranean Journal of Chemistry 10, no. 8 (November 2, 2020): 809. http://dx.doi.org/10.13171/mjc10802011021539st.

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<p>Wadi El Reddah representing a semi-closed basin, extends in the N-S direction. It has only one outlet at the northern tip while the wadi collects floodwater from internal tributaries along wall rocks. The present study discusses the relationship between geology and geochemistry data to detect anomalous radioactive locations. The geochemical maps show the mineralization areas with abnormal rare metal contents. This led to two uranium occurrences (GXXIII and GXXIV) at Gabal Gattar in the perthitic leucogranite. At Wadi El Reddah, high contents of pathfinder elements (REE, Y, Zn, Nb and As) were discovered at the southern and eastern boundaries. This may be attributed to the presence of alkali feldspar granite at Gabal Gattar at the upstream of Wadi El Reddah and also to the sharp contact between Gabal Gattar and Hammamat Sedimentary rocks. A strong positive correlation coefficient between Fe<sub>2</sub>O<sup>t</sup> and or Al<sub>2</sub>O<sub>3</sub> with Zr, Hf, Nb, Ta, REE, U, Rb, and Th reflects their association with thematization processes.</p>
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7

McMahon, David. "The Turin Papyrus Map The Oldest Known Map with Geological Significance." Earth Sciences History 11, no. 1 (January 1, 1992): 9–12. http://dx.doi.org/10.17704/eshi.11.1.484472n43765605k.

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The Turin papyrus map is over 3000 years old. More than 100 years of study mainly by egyptologists and by some geologists demonstrate that it shows workings in a known ancient mining and quarrying district of Upper Egypt (the Wadi Hammamat). It seems to have been made in connection with the transportation (and damage?) of a statue from the quarries. The map is significant because of its antiquity and because it shows substantial geological information which underlies the mining and quarrying knowledge which it contains.
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8

Steiner, Richard C. "The Scorpion Spell from Wadi Hammamat: Another Aramaic Text in Demotic Script." Journal of Near Eastern Studies 60, no. 4 (October 2001): 259–68. http://dx.doi.org/10.1086/468948.

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9

Proussakov, Dimitry B. "ЗАГАДКИ ДОДИНАСТИЧЕСКОЙ ПЕТРОГЛИФИКИ С ПОПРАВКОЙ НА КЛИМАТ И ГИДРОЛОГИЮ: ЛОДКИ (И РЕКИ?) В ВЕРХНЕЕГИПЕТСКИХ ВОСТОЧНЫХ ВАДИ." Journal of the Institute of Oriental Studies RAS, no. 4 (14) (2020): 20–42. http://dx.doi.org/10.31696/2618-7302-2020-4-20-42.

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Prehistoric rock drawings of large boats in wadis of the central Eastern Desert, Egypt, divided their investigators into two main groups with quite different views about their origins and cultural affiliation. One of the groups (P. Červiček et al.) insisted on ‘religious’ (cultic, magic, etc.) nature of these petroglyphs attributing them to local traditions but actually tearing away from the reality, primarily on the ground that boats could have never come to be in the desert many tens of kilometers from both the Nile and the Red Sea. Another one, following ideas of W. M. Flinders Petrie, interpreted these boat images as ships of a ‘Dynastic Race’ of oversea invaders who conquered Egypt and consolidated her under their power. This hypothesis, once disapproved by most of archaeologists and Egyptologists, has recently acquired many new adherents; it assumes, in particular, the most real rivers to have flown at the time of the earliest boat petroglyphs (5th to 4th Millennia B.C.) along Wadi Hammamat and Wadi Barramiya, where short routes pass from the Red Sea coast to the Nile. Even rejecting Petrie’s ‘diffusionistic’ version on the whole, one cannot ignore the palaeogeographical fact that the climate of Predynastic Egypt was moist, characterized by monsoon rains which, in combination with geomorphology of the Eastern Desert, could only have favoured here in the period under consideration the formation of regular tributaries of the Nile.
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10

González-Tablas Nieto, Javier. "Quarrying Beautiful Bekhen Stone for the Pharaoh: The Exploitation of Wadi Hammamat in the Reign of Amenemhat III." Journal of Egyptian History 7, no. 1 (August 18, 2014): 34–66. http://dx.doi.org/10.1163/18741665-12340013.

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The greywacke quarries in Wadi Hammamat are one of the best known examples of this kind of activity due to the number of inscriptions preserved at the site. Although a number of approaches to these inscriptions have been made, it is quite usual to find general studies about epigraphic features or the activities of one important functionary. The aim of this paper is to focus on the royal activities in the quarries at the end of the Middle Kingdom, more precisely in the reign of Amenemhat III, analyzing for that purpose both epigraphic and comparative archaeological data, in order to build a comprehensive image of the Egyptian works at this quarrying site.
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11

Goelet, Ogden. "wʒḏ-wr, Punt, and Wadi Hammamat: The Implication of Verbs of Motion Describing Travel." Abgadiyat 11, no. 1 (May 12, 2016): 51–56. http://dx.doi.org/10.1163/22138609-90000042.

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12

نصیر, أحمد عبدالله. "Geoarchaeological study on Rock Art Sites, With Special Emphasis on Gabel-EL-Silsilah and Wadi Hammamat." مجلة کلیة الآداب بقنا 7, no. 7 (September 1, 1997): 5–60. http://dx.doi.org/10.21608/qarts.1997.113843.

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13

Mouhareb, R. S. "Petrographical and mineralogical studies of Hammamat sediments and Gattarian granite along Wadi Belih, north Eastern Desert, Egypt." Journal of Petroleum and Mining Engineering 19, no. 1 (December 1, 2017): 63–70. http://dx.doi.org/10.21608/jpme.2017.39124.

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14

Szaniawska, Lucyna. "Geological content on maps and in accompanying texts developed until the end of the 18th century." Polish Cartographical Review 49, no. 2 (July 1, 2017): 79–91. http://dx.doi.org/10.1515/pcr-2017-0007.

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Abstract For many centuries on general geographical maps and early maritime maps geological information was rarely included. The map of the Wadi Hammamat valley, the Borgia world map, the Catalan world map and Carta de nauigar per le Isole nouamente... portolan chart were indicated as examples. Places where minerals occurred were presented mainly using textual descriptions. Among Renaissance maps and later maps published before the second half of the 18th century, the map of the Kingdom of Bavaria by Philipp Apian and the map of the Duchy of Świdnica in Silesia by Johann Wieland and Matthaus Schubart were discussed as examples. Distribution of raw materials and places of their extraction were shown using simple geometric signs with graphic characteristics for a given period. Mineralogical maps published in the second half of the 18th century were described based on the example of maps by Jean-Étienne Guettard and Johann Jirasek. Their content was compared with the texts accompanying them, developed under patronage of the contemporary scientific institutions and relevant methods of geological information presentation were described. From the late Renaissance symbols signifying extraction sites of raw materials had simplified and rather random shapes which indicates ‘unhurried’ development of cartographic methods on geological maps.
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15

El-Rahman, Yasser Abd, Ali Polat, Brian J. Fryer, Yildrim Dilek, Mohamed El-Sharkawy, and Shawki Sakran. "The provenance and tectonic setting of the Neoproterozoic Um Hassa Greywacke Member, Wadi Hammamat area, Egypt: Evidence from petrography and geochemistry." Journal of African Earth Sciences 58, no. 2 (September 2010): 185–96. http://dx.doi.org/10.1016/j.jafrearsci.2010.02.010.

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16

Fowler, A., and M. M. Abdeen. "Reappraisal of strain estimations and measurement methods in the Hammamat Group sediments: Comparison of primary and secondary grain fabrics with new data from Wadi Zeidun and Wadi Arak basins, CED, Egypt." Precambrian Research 247 (July 2014): 1–32. http://dx.doi.org/10.1016/j.precamres.2014.03.009.

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17

Khalaf, Ezz El Din Abdel Hakim. "Mechanisms of volcaniclastic aggradation in fluvial systems influenced by explosive volcanism: An example from Neoproterozoic Hammamat Group, Wadi Queih area, Central Eastern Desert, Egypt." Journal of African Earth Sciences 68 (June 2012): 44–66. http://dx.doi.org/10.1016/j.jafrearsci.2012.03.010.

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18

Anketell, J. M., and S. M. Ghellali. "Stratigraphic Relationships of Basalt Lava Flows to the Pleistocene Sedimentary Sequence of the Mizdah Region, Tripolitania, S.P.L.A.J." Libyan Studies 21 (1990): 61–63. http://dx.doi.org/10.1017/s0263718900001473.

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AbstractCalcreted debris flow breccias which form the lowermost Pleistocene deposits in the Hammadah Al Hamrah region are locally overlain by well cemented conglomerates of the Old Wadi Terraces. These are commonly capped by a younger, mature calcrete which is also found patchily developed on the Tertiary and Mesozoic limestone bedrock. Basalt lava flows rest either on an eroded surface in the conglomerates or directly on the debris flows; however, their relationship to the younger calcrete is rarely seen. In the area north-east of Mizdah a pre-younger calcrete age for the basalts is proposed on the basis of calcrete-filled fissures which invade the topmost part of the lava sequence. Similarity of the Mizdah sequence to that at Wadi Ghan in the Jabal Nafusah supports correlation of the conglomerates and basalt with Unit Q2 and the younger calcrete event with the upper calcrete of the Jifarah/Wadi Ghan areas. The calcreted breccia/debris flow deposits in turn correlate with Unit Q1 and the lower calcrete.
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19

Imam, Mostafa M., and Ahmed A. Refaat. "Stratigraphy and facies analysis of the Miocene sequence at Gabal Hammam Sayidna Musa and Wadi Abura, southern Sinai, Egypt." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2000, no. 7 (July 14, 2000): 385–408. http://dx.doi.org/10.1127/njgpm/2000/2000/385.

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20

Hamlat, Abdelkader, Azeddine Guidoum, and Imen Koulala. "Status and trends of water quality in the Tafna catchment: a comparative study using water quality indices." Journal of Water Reuse and Desalination 7, no. 2 (March 30, 2016): 228–45. http://dx.doi.org/10.2166/wrd.2016.155.

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Water quality indices (WQIs) are necessary for resolving lengthy, multi-parameter, water analysis reports into single digit scores; different WQIs have been developed worldwide which are greatly differing in terms of mathematical structures, the numbers and types of variables included, etc. The aim of this paper is to evaluate trends of water quality in Tafna basin with a comparison of 10 WQIs perceived as the most important indices for water quality assessment. The results show that there is an appreciable difference between indices values for the same water sample. The results also show that water quality categorization for sampling stations in the Canadian Council of Ministers of the Environment WQI (CCMEWQI) and British Columbia WQI (BCWQI) was found to be ‘marginal’ for all sampling stations, except Hammam Boughrara reservoir and Mouillah wadi where it was found to be ‘poor’. For the Aquatic Toxicity Index, it was found to be ‘totally unsuitable for normal fish life’ for all stations and ‘suitable only for hardy fish species' for Mouillah wadi and Boughrara reservoir. The results show that this transboundary catchment always needs strategies for more effective pollution control management. Future use of WQIs in this way should prove a valuable tool for environmental planning decision-makers in tracking water quality change.
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21

Gliz, Mohamed, Boualem Remini, Djamel Anteur, and Mohammed Makhlouf. "Vulnerability of soils in the watershed of Wadi El Hammam to water erosion (Algeria)." Journal of Water and Land Development 24, no. 1 (March 1, 2015): 3–10. http://dx.doi.org/10.1515/jwld-2015-0001.

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Abstract Located in the north west of Algeria, the watershed of Wadi El Hammam is threatened by water erosion that has resulted the silting of reservoirs at cascade: Ouizert, Bouhanifia and Fergoug. The objective of this study is to develop a methodology using remote sensing and geographical information systems (GIS) to map the zones presenting sensibility of water erosion in this watershed. It aims to produce a sensibility map that can be used as a reference document for planners. The methodology presented consists of three factors that control erosion: the slope, the friability material and the land use, which were integrated into a GIS. The derived erosion sensibility map shows three areas of vulnerability to water erosion: low, medium and high. The area of high vulnerability corresponds to sub-basin of Fergoug.
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22

Peterson, Jane. "Khirbet Hammam (WHS 149): A Late Pre-Pottery Neolithic B Settlement in the Wadi el-Hasa, Jordan." Bulletin of the American Schools of Oriental Research 334 (May 2004): 1–17. http://dx.doi.org/10.2307/4150103.

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23

Djellouli, F., A. Bouanani, and K. Babahamed. "Climate change: assessment and monitoring of meteorological and hydrological drought of Wadi El Hammam Basin (NW- Algeria)." Journal of Fundamental and Applied Sciences 8, no. 3 (March 14, 2018): 1037. http://dx.doi.org/10.4314/jfas.v8i3.20.

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24

Anketell, J. M. "Quaternary Deposits of Northern Libya — Lithostratigraphy and Correlation." Libyan Studies 20 (January 1989): 1–29. http://dx.doi.org/10.1017/s0263718900006567.

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In recent years basic regional geological mapping of northern Libya by the Industrial Research Centre, Tripoli, together with the UNESCO Libyan Valleys Survey of eastern Tripolitania and the work of the author and Dr S. M. Ghellali in the Jifarah Plain and Jabal Nafusah, have greatly added to our knowledge of Quaternary deposits in the region. This work is described and evaluated against the background of earlier studies. The succession of major depositional, soil forming and erosional events which characterise the fluvio-aeolian deposits of the Jifarah Formation can be recognised in, and thus used to subdivide, laterally equivalent aeolianite, fangravel and wadi gravel deposits in the Jifarah Plain. Comparisons of this succession with others from throughout the region indicate that the events are of regional significance and that the Jifarah sequence provides a sound framework for lithostratigraphic correlation and a basis for facies analysis and chronostratigraphic studies.This review is largely limited to the northern margins of Libya north of the 30th parallel (Fig. 1). It is convenient to subdivide the zone into several regions. These are:(a) The Jifarah Plain and foothills of the Jabal Nafusah.(b) The Hammada Al Hamra Plateau and major valleys of eastern Tripolitania.(c) The coastal region from Misratah to Ajdabiyah.(d) Cyrenaica from Soluq to Al Bardia.
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25

Belaroui, Abdelhakim, Fatima Zohra Haouchine, and Abdelhamid Haouchine. "Rainfall-runoff modeling: flow characterization of Hammam Melouane Wadi Algeria." Arabian Journal of Geosciences 12, no. 15 (August 2019). http://dx.doi.org/10.1007/s12517-019-4610-y.

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26

Aghaei, Mehrdad, and Farshid Hadi. "MYSTICAL SPARKS IN THE SAHIFEH SAJADIEH AND ITS STRATEGIC ROLE IN ISLAMIC MYSTICISM." Gênero & Direito 8, no. 5 (October 28, 2019). http://dx.doi.org/10.22478/ufpb.2179-7137.2019v8n5.48666.

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Sahifah Sajjadiyah as the first influence of the infallible prayer on the darkness of polytheism and mysticism, this legacy of the infallible Imam is a special and unique book containing prayers to Imam Sajjad (PBUH), full of ethical and mystical themes. , Like a beacon of light for seekers of the path of Islamic righteousness, and as a home for the mystics of the Vale and the guidance of the lost mystics in the Wadi. This study aims to analyze and analyze the monotheistic and mystical doctrines of the Sajadiyyah by descriptive-analytic method, and to examine the reason for the prayerfulness of this Bible as well as the monotheism from Imam Zayn al-Abidine's viewpoint and the path of Islamic mysticism. It has been studied and studied in Sahifah, as the Sahajadiyah is regarded as the primary basis for the foundation of the Islamic mysticism and the monotheistic way of life, and it can certainly play a key strategic role in Sahifah. The Imam (PBUH) deals with Islamic mysticism and its positive reflections in this field and refers to that Imam Hammam as Imam al-Abidin and Mersdal Elkin and Alarfyn introduced to the world
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